2023
DOI: 10.1016/j.rines.2023.100001
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Relicts of Neo-Tethyan mantle wedge in the Indo-Burma Range, India: Record of carbonate metasomatism and Neo-Tethyan mantle evolution

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Cited by 5 publications
(3 citation statements)
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“…A fully nonlinear inversion is applied to determine the causative body by inverting ground deformations and gravity variations due to pressure and mass anomalies implanted into an elastic medium. Impressive outcomes are in volcanic environments, where ground deformations by seismic sequences are associated with over-pressured magmatic geobodies (Camacho et al, 2020;Cammarata et al, 2018;Cintorrino et al, 2019;Dhawale et al, 2023;Kianoush et al, 2023e;Kianoush et al, 2024;Kianoush et al, 2023b;Kingson et al, 2023;Kwami et al, 2023;Palano et al, 2023;Pirhadi et al, 2023). In this research, a 1-D inversion problem, also known as the pseudo-well problem, has been investigated.…”
Section: Introductionmentioning
confidence: 99%
“…A fully nonlinear inversion is applied to determine the causative body by inverting ground deformations and gravity variations due to pressure and mass anomalies implanted into an elastic medium. Impressive outcomes are in volcanic environments, where ground deformations by seismic sequences are associated with over-pressured magmatic geobodies (Camacho et al, 2020;Cammarata et al, 2018;Cintorrino et al, 2019;Dhawale et al, 2023;Kianoush et al, 2023e;Kianoush et al, 2024;Kianoush et al, 2023b;Kingson et al, 2023;Kwami et al, 2023;Palano et al, 2023;Pirhadi et al, 2023). In this research, a 1-D inversion problem, also known as the pseudo-well problem, has been investigated.…”
Section: Introductionmentioning
confidence: 99%
“…A fully nonlinear inversion is applied to determine the causative body by inverting ground deformations and gravity changes due to pressure and mass anomalies embedded into an elastic medium. Interesting results are in volcanic environments, where ground deformations by seismic sequences are related to over-pressured magmatic bodies (Camacho et al, 2020;Cammarata et al, 2018;Cintorrino et al, 2019;Dhawale et al, 2023;Kianoush et al, 2023b;Kingson et al, 2023;Palano et al, 2023). The rock physics model links the physical parameters with elastic properties and can serve as a constraint for seismic methods (Chen et al, 2023;Yuan et al, 2022).…”
Section: Introductionmentioning
confidence: 99%
“…Consequently, a numerical approach shall be considered to solve for these unknowns under specific initial and boundary conditions. Advanced numerical schemes, e.g., the finite element method, are suitable for solving complex geomechanical problems (Ebrahimabadi et al, 2015;Hosseini et al, 2023a;Hosseini et al, 2023b;Kianoush et al, 2023c;Kingson et al, 2023;Mackerle, 1999;Motahari et al, 2022;Palano et al, 2023;Rafieepour et al, 2020;Tao and Ghassemi, 2007;Zalnezhad et al, 2022). Regardless, the finite element method is time-consuming and computationally expensive.…”
Section: Introductionmentioning
confidence: 99%